Characterization of magma from inclusions in zircon: Apatite and biotite work well, feldspar less so

Geology

Volumn 39, Issue 9, 2011, Pages 863-866

  Jennings, E S ^a   Marschall, H R ^a,b   Hawkesworth, C J ^c   Storey, C D ^d  

^a UNIVERSITY OF BRISTOL   (United Kingdom)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c UNIVERSITY OF ST ANDREWS   (United Kingdom)

^d UNIVERSITY OF PORTSMOUTH   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

ALKALI FELDSPAR; ANTARCTICA; BULK ROCKS; CHEMICAL COMPOSITIONS; CRUSTAL EVOLUTION; DETRITAL ZIRCON; DETRITAL ZIRCON GRAINS; DIFFERENTIATION PROCESS; HIGH CONCENTRATION; HOST ROCKS; LOW CONCENTRATIONS; MATRIX; MINERAL INCLUSIONS; PLUTONIC ROCKS; POTENTIAL SOURCES; RELATIVE ABUNDANCE; SEDIMENT PROVENANCE;

ANOXIC SEDIMENTS; APATITE; FELDSPAR; IGNEOUS ROCKS; MICA; ROCKS;

ZIRCON;

APATITE; BIOTITE; CHEMICAL COMPOSITION; CRUST-MANTLE BOUNDARY; CRYSTALLIZATION; FELDSPAR; IGNEOUS INTRUSION; MAGMA; PLAGIOCLASE; SOURCE ROCK; ZIRCON;

ANTARCTICA; EAST ANTARCTICA; QUEEN MAUD LAND;

EID: 80053954586     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G32037.1     Document Type: Article

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